河南省钼矿床赋存特征  

THE OCCURING CHARACTERISTICS OF MOLYBDENUM ORE DEPOSIT IN HENAN

作　　者：李云 王文娟[2] 郭锐[2] 王秋云[2] 吴飞[2] 付治国[2] 

机构地区：[1]郑州工业贸易学校,河南郑州450007 [2]河南省地质矿产勘查开发局第二地质勘查院,河南许昌461000

出　　处：《中国钼业》2007年第3期10-13,共4页China Molybdenum Industry

摘　　要：通过对河南省钼矿床赋存特征的分析研究,总结出如下规律:1)河南省钼矿床属东秦岭-大别山钼成矿带的一部分;2)在地槽活动带的边缘区,构造岩浆岩带是钼矿床产出的有利场所;3)成矿母岩是主要控矿因素,同时也是最重要的找矿标志;4)区域巨大的燕山期花岗岩基是成钼小岩体的母岩,而成钼小岩体又是钼矿床的成矿母岩,三者在空间分布上具有高度的一致性。By analysing thd occuring characteristics of Henan molybdenum ore deposit, the following laws are summarized：the Henan molybdenum ore deposit is the part of the east Qinling - Dabie mountain molybdenum ore - forming belt;2） The structure mag ma belt in the edge of geosyncline active zone is beneficial place in which the molybdenum ore deposit produce; 3） The ore - forming mother rock is the main ore - controlling same time it is the most important ore - forming marking;4 ） the regional huge Yanshan granite mother rock of molybdenum forming small rock body, which also is the ore - forming mother rock ore deposit. These three have high consistence in the space.

关 键 词：钼矿床 地质特征 赋存特征 

分 类 号：P618.65[天文地球—矿床学]